01 mass spectrometry 101 final hofstadler
TRANSCRIPT
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Disclaimer
This presentation covers the basic concepts ofmass spectrometry
The material is not specifically required to operate
the Ibis T5000
Users are not expected to tune and/or optimize themass spectrometer
The goal of this presentation is to give the user abasic understanding of where/how massspectrometry fits into the Ibis workflow
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Overview
Introduction what is Mass Spectrometry? Mass Spectrometry (MS) and Ibis T5000
Brief History
General Components
The Mass Spectrum Definitions and Nomenclature
Ionization Sources
Matrix Assisted Laser Desorption Ionization (MALDI)
Electrospray Ionization (ESI) Others
Time-of-Flight (TOF) Mass Analyzers
ESI-TOF of nucleic acids
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Mass Spectrometry and Ibis platform
Profile 1
Profile 2
Profile 3
Forensic profile compared with existing databaseentries, or used to populate database
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Mass Spectrometry of Nucleic Acids?
Information content From precise mass measurements unambiguous basecompositions are derived [A10 G23 C32 T17] = [10 23 32 17]
Speed < 1 minute/sample
Applicability to mixtures Dynamic range is around 100:1 MS succeeds where sequencing fails (e.g. mixtures)
Automation End-to-end process is highly automated (including spectral
processing/interpretation)
Sensitivity Single copy detection demonstrated with PCR front-end
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What is a Mass Spectrometer?
An instrument which measures the mass-to-charge ratio(m/z) of ionized analyte based on its response to appliedelectric and/or magnetic fields
atoms, molecules, clusters, and macromolecularcomplexes
The m/zmeasurement is converted to a mass measurement mis in atomic mass units or Daltons (Da)
1 Da = 1/12 the mass of a single atom of 12C
1 Da = 1.66 x 10-24 grams
zis an integer multiplier of the fundamental unit of charge
(q) q = 1.602 x 10-19 Coulombs
Mass = m/z X z
A mass spectrometer is essentially a molecular (or atomic)scale that weighs analytes of interest
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Brief History 1897 J.J. Thompson announced the presence of electrons or
corpuscles based on the deflection of cathode rays byelectric and magnetic fields
He later used this beam-deflection device to measure themass of the electron (1906 Nobel Prize)
+ -
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Brief History (cont.) 1919 F. W. Aston used Thompsons mass spectrometer to
measure the atomic masses of 30 gaseous elements andprove the existence of multiple isotopes. Relative abundancemeasurements were made by recording isotope lines on film.Mass spectroscopy Nature1919; 104; 393. (1922 NobelPrize)
Design principles are the basis of modern electric and magneticsector instruments
Astons original Positive-Ray Mass Spectrograph
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Basic Components
Inlet System
sample introduction
Ion Sourceionizes sample
Ion Analyzersort ions by m/z
Ion Detectorcounts ions
Data Systemsignal processor
Mass Spectrum
Vacuum chamber
Instrument Control Computercontrols timing and voltages
ionoptics
ionoptics
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The Mass Spectrum
300 400 500 600m/z
RelativeAbun
dance
ArbitraryIntensity
DetectorResp
onse
100
50
0
25
75
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The Mass Spectrum
/disk2/data/12_4/628_23426/11/pdata/1xspec MonDec 7 19:16:471998
200 300 400 500 600m/z
397.13 397.18
C15H16F6N4O2397.1104
C19H22N6O4397.1628
(M-H)-
M/M > 75,000
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The Isotopic Envelope
Most elements have more than 1 isotope
For a given atom type, different isotopes havedifferent numbers of neutrons e.g. an atom of 12C has 6 neutrons, 6 protons, and 6
electrons an atom of 13C has 7 neutrons, 6 protons, and 6
electrons
The mass of a neutron is 1.00867 Da
Each element has different numbers and relativeabundances of other isotopes: 12C = 98.90% 13C = 1.10% 35Cl = 75.77% 37Cl = 24.23% 19F = 100%
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The Isotopic Envelope
Unless a molecule is composed of onlymonoisotopic elements, there is a finite probabilitythat it will contain one or more heavy isotopes
The relative abundance of the monoisotopic peak
decreases with increasing mass Observed distribution is the sum of isotopic
contributions from all hetero-isotopes
Except in a few cases, isotopic fine structurecannot be resolved e.g. for an N+2 peak the contributions from 2 13C and 1 18O
cannot be resolved
Consider carbon clusters:
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Isotope Distributions of Carbon
8.0106 12.010 16.009 20.009
C1
MW
1193.1 1197.1 1201.1 1205.1 1209.1
C100
MW
11979 11995 12011 12027 12043
C1000
MW
12C = 100%
13C = 1.1%
12C = 89.1%
13C = 100%
213C = 54.6%
12C = 0.01%
1113C = 100%
2013C = 3.9%
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Definitions and Nomenclature Resolution : M/M
actually (m/z)/(m/z) (m/z) : peak width at full width half maximum (FWHM)
0
33
66
100
1201.8 1203.8 1205.8 1207.8 1209.8
m/z
r
t
m/z = 1.20
RelativeAbundanc
e
Resolution (FWHM) = 1205.8
1.20= 1005
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Definitions and Nomenclature
Resolution (cont.) can be limited by the inherent width of the isotope envelope
step function to isotopic resolution
need M/M > molecular weight for isotopic resolution
0
33
66
100
1201.8 1203.8 1205.8 1207.8 1209.8m/z
r
t
m/z = 0.12
RelativeAbundance
Resolution (FWHM) = 1205.240.12
= 10044
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Definitions and Nomenclature:Mass Measurements3 ways to specify molecular weight
Monoisotopic Molecular Weight
All 12C, 14N, 16O, etc.
most accurate method for low
MW species
monoisotopic peak is base peak(i.e. most abundant peak) up to
about 2 kDa
Average Molecular Weight
most commonly used
few MS platforms can resolve
isotopes for analytes > 5 kDa between monoisotopic and
average increases with increasing MW
MWmi
MWave
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Definitions and Nomenclature:Mass Measurements (cont.)3 ways to specify molecular weight
Most Abundant Isotope Molecular Weight
not widely used
convenient for high MW, isotopically resolvedspecies
24622 24638 24654 24670 24686
C780 H981 N300 O478 P79
mass
MWmost abundant isotope
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Definitions and Nomenclature
Mass Measurement Accuracy|(m/z)theory - (m/z)measured|
(m/z)theory= Mass Measurement Error (ppm)
cmpd Mcalc Mmeas m ppmC15H16F6N4O2 397.1105 397.1104 0.0001 0.25C19H22N6O4 397.1630 397.1628 0.0002 0.50
397.13 397.18
C15
H16
F6N
4O
2397.1104
C19H22N6O4397.1628
(M-H)-
M/M > 75,000
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Mass Spectrometry Nuts and Bolts
Ionization Sources
Mass Analyzers
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Ionization Sources
Ionization is the process by which analytes arecharged
Adding or removing electrons (e-) (MW = 0.0006 Da)
Adding or removing protons (H+) (MW = 1.0078 Da)
Several very effective methods for ionizing lowmolecular weight and/or volatile compounds.Limited MS to analytes with molecular weightsunder ~1 kDa
In the 1980s, two ionization methods developedfor ionizing high molecular weight analytes
MALDI & ESI
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Ionization Sources for Low MW Analytes
APCI Atmospheric Pressure Chemical Ionization formation of analyte ions through charge exchange with
ionized carrier gas
EI Electron Ionization generation of ions by bombarding gas phase molecules
with high energy electrons analyte must be volatile
ionization energy dictates
extent of fragmentation
still widely used w/ GC
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laser
Ionization Sources - MALDI Matrix Assisted Laser Desorption Ionization
Sample is co-crystallized with a matrix which absorbsphotons and creates a desorption plume that ionizes thesample
Gentle ionization technique (harsher than ESI)
A pulsed ion source Produces singly charge ions
Relatively salt tolerant
Effective for wide range of MWs
Fast and automatable
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Ionization Sources - ESI Electrospray Ionization
Ions are desolvated/desorbed from highly charged liquid droplets
Generates multiple charge states of large analytes
results in folded-over spectra which can be recorded over narrower m/zrange
Very soft ionization technique
applicable to labile molecules and noncovalent complexes
Low tolerance for nonvolatile salts, buffer additives, and detergents
rigorous sample clean-up required for some applications
High sensitivity
applicable to analyte concentrations < 100 nM
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A Negative Ionization Mode ESI Mass Spectrumof a Low MW Analyte: Singly Charged Spectrum
Well A03
Q:\roboticsdata\archive\completed\P00005666\3\acqus
477.07 587.09 708.52 841.36 985.6 1141.25 1308.3 1486.76 1676.63 1877.9 2090.58
m/z
0.00
4648
9296
13944
18592
m/z= 1347.10
MW = 1347.10 + MWproton= 1348.11 Da
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(M-H+)1-
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An ESI (+) Mass Spectrum of a High MW Analyte(Carbonic Anhydrase Protein MW = 28,821 Da)
What dont we know:Molecular Weight?
Which Charge States?What are all these peaks?
What do we know:m/zof lots of peaksAdjacent peaks differ by 1 charge
700 800 900 1000m/z
1100
RelativeInt
ensity
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Conventional Deconvolution of ESI-MS Spectrum
700 800 900 1000m/z 1100
RelativeIn
tensity
From m/z of peaks and z, calculate z of one peak.
961.7 = m/z1
994.8 = m/z2
m/z1 m/z2
m/z2= z1
33.1
994.8= z1= 30
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700 800 900 1000m/z
1100
RelativeIn
tensity
961.7 (M+30H+)30+
MW = (961.7 x 30) (30 x 1.0078)= 28,821 Da
accuracy improved by averagingacross multiple (all) charge states
Conventional Deconvolution of ESI-MS SpectrumUse zand m/zto calculate mass
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ESI-MS of DNA
Phosphodiester backbone iseasily deprotonated at high pH
ESI most effective in negativemode (in positive ionizationmode basic groups on bases areprotonated)
Both backbone and nucleobaselinkages to sugar are relativelylabile
We have optimized solution andinterface conditions for DNAanalysis by mass spectrometryover the past 10 years
HO
N
NN
N
NH2
O
HO
HH
HH
PO
O
O-
N
NH2
ON
O
HO
HH
HH
PO
O
O-
NH
N
N
O
NH2N
O
H
HH
HHO
PO
O-
O-
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Then and NowThen (1981)
Pre-contributions of Fenn,Tanaka, Hillenkamp/Karas
20-mer DNA
Cf252 desorption - TOF
M/M ~ 25 MW = 6301 + 5 (~ 800 ppm)
Now
Additional contributionsfrom Marshall,McLafferty, McLuckey,Smith and others
120-mer DNA acquired infully automated modality
ESI-FTICR
M/
M = 150,000 MW = 37,091.18 + 0.04
~ 1 ppm
1001.0 1002.0 1003.0 1004.0
(M-37H+)37-
900 1000 1100m/z
1200
*
43-
41-
39- 37-
35-
33-
31-
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An ESI Mass Spectrum of a PCR Productdoublet peaks at each charge state correspond to
forward and reverse strands of amplicon
800 900 1000 1100 1200 1300m/z
33-31-
29-
27-
25-
35-
37-
39-
41-
800 900 1000 1100 1200 1300m/z
33-31-
29-
27-
25-
35-
37-
39-
41-
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Raw ESI-MS spectrum from 3-plex PCR mix
Internalmass
calibrant
Internalmass
calibrant
Internal mass calibrants bracketthe spectrum for accurate
calibration of the measurementsbefore deconvolution
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Deconvolved ESI-MS spectrum from 3-plex PCR
30,000 32,000 34,000 36,000 38,000 40,000 42,000 44,000
0
1000
2000
3000
4000
5000
6000
Mass (Da)
Signalintensity
3285
5.1
34143.8
37058
.2
37254.2
42162.1
42710
.3
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Masses to Base Composition
Requires 25 ppmmass measurement error
Math takes into accountWatson-Crick base pairing
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Microsoft Media Elements
Microsoft Media Elements
Microsoft Media Elements
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Masses to Base Composition
Require masses of both strands and fact that thestrands are complimentary to determine basecomposition
Single Strand: 32889.450 Da
(+ 25 ppm or 0.75 Da): 928 base comps(+ 1 ppm or 0.03 Da): 82 base comps
Single Strand: 33071.462 Da(+ 25 ppm or 0.75 Da): 948 base comps
(+ 1 ppm or 0.03 Da): 95 base comps
ppm: part per millionDa: Dalton (atomic mass unit)
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Exact Mass Measurements of Both Strands FacilitatesUnambiguous Base Composition Determination
ppm0-2550
100250500
# comp pairs1
13
663781447
AwGxCyTz
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Mass Measurement and the Canadian Nickel
Penny = 2.500 g
Nickel* = 3.950 gDime = 2.268 g
Quarter = 5.670 g
A = 313.0576 amuG = 329.0526 amu
C = 289.0464 amu
T = 304.0461 amu
The Coins and Scale analogy doesnt work if
using all US coins as a US Nickel weighs 5.000 g Thus 5 g could be two pennies or one nickel
Interesting parallel to nucleobases with massmeasurement error
A mass shift of 15 + 1 Da could be a A -> G ora C -> T
A double SNP A -> G and T-> C would result ina 1 Dalton difference
A one Dalton uncertainty is consistent withtwo base compositions
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Microsoft Media Elements
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Mass Measurement and the Canadian Nickel
Penny = 2.500 g
Nickel* = 3.950 gDime = 2.268 g
Quarter = 5.670 g
A = 313.0576 amuG = 329.0526 amu
C = 289.0464 amu
T = 304.0461 amu
The Coins and Scale analogy doesnt work ifusing all US coins as a US Nickel weighs 5.000 g
Thus 5 g could be two pennies or one nickel
Interesting parallel to nucleobases with massmeasurement error
A mass shift of 15 + 1 Da could be a A -> G ora C -> T
A double SNP A -> G and T-> C would result ina 1 Dalton difference
A one Dalton uncertainty is consistent withtwo base compositions
We have a Canadian Nickel nucleobase
13C labeled guanosine shifts the mass by 10Da per incorporation
No confusion over which SNP is present
No uncertainty as to whether the A/G T/Cdouble SNP is present
G = 339.1662
Microsoft Media Elements
Microsoft Media Elements
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881.5 883.14 884.79 886.43 888.08 889.73 891.38 893.03 894.69 896.34 898m/z
A48 G18 C31 T40
A47 G19 C32 T39
42030.19 Da42478.39 Da
42031.18 Da42479.38 Da
Without mass tag:Product strands differ by 1 Da for two products that differ by a GA and CT SNP atthe same time.
Some double SNPs cause small mass differences
High mass precision and mass tag combine to provideunambiguous base compositions in routine operation
Microsoft Media Elements
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With mass tag:
With 13C-dGTP, the mass separation increases to ~10 Da for each strand
Correspondinguntagged peaks
=
881.5 883.14 884.79 886.43 888.08 889.73 891.38 893.03 894.69 896.34 898m/z
A48 G18 C31 T40
A47 G19 C32 T39
42187.02 Da
42694.04 Da
42197.81 Da42704.83 Da
Mass tag increases mass separation for theseSNPs
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30,000 32,000 34,000 36,000 38,000 40,000 42,000 44,0000
1000
2000
3000
4000
5000
6000
Mass (Da)
Signalinten
sity
32855.1
34143.8
[A40 G9 C40 T19]
37058.2
37254.2
[A47 G18 C25 T30]
42162.1
42710.3
[A49 G17 C31 T40]
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Size Constraints
We generally characterize PCR products < 150 bp(~47 kDa/strand)
In general, 25 ppm mass measurement error or
better will provide unambiguous base compositionfor double stranded products < 150 bp
Analysis of larger products is feasible, but
information content is lower Spectra more congested
Math not in our favor
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700 900 1100 1300 1500 1700 1900 m/z
2000
4000
6000
8000
10000
12000
a.i.
91000 92000 93000 94000 mass
Meas. MWave = 91009.4
Theo. MWave = 91008.7ppm error = 7.7
Meas. MWave = 93601.9
Theo. MWave = 93601.0
ppm error = 9.6
(M-100H+)100-
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Number of possible base compositions asa function of ppm mass error and mass
ppmError
SS1 SS2DS
MWave=91008.7 MWave=93601.0
1 2563 2580 1
5 12846 14296 3
10 25809 29054 10
20 * x x 62
25 x x 89
50 x x 367
*Average ESI-TOF error over 24 replicates of 299-mer
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ESI Parameters Ion desolvation is controlled by several parameters
Temperature of desolvation gas
Capillary-skimmer potential difference
Pressure in capillary-skimmer interface region
Excessive activation in the interface region can lead to dissociation
DNA is labile relative to proteins and one must use gentleinterface conditions
skimmercone
rf-only hexapole
gateelectrode
inletcapillary
turboPump
ESIplume
roughpump
turbodragpump
coldcathodegauge
heatedcounter-current
gasflow
To MS
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Solution/Desolvation Conditions(same sample analyzed under different source conditions)
ESI-TOFPCR product from E. Colidetected as single strands
ESI-TOFPCR product from E. Colidetected as intact duplex
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Effect of Capillary-Skimmer Potential Difference20-mer phosphorothioate oligonucleotide
(M-6H+)6-
(M-4H+)4-(M-8H+)8-
(M-6H+)6-
(M-4H+)4-(M-8H+)8-
500 700 900 1100 1300 1500m/z
1700500 700 900 1100 1300 1500m/z
1700
w3(1-)
a4-base(1-)
a4(1-)
w3-A-H2O(1-)
a3-base(1-)
Vcap = -54 V
Vcap = -128 V
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Salt is a Killer
Nonvolatile counterions (e.g. Na+
, K+
, Mg2+
, etc) arenot removed during desolvation High concentrations can preclude the generation of a
stable ESI plume
Oligonucleotides are more vulnerable tocontamination than proteins Phosphodiester backbone is highly anionic
Larger oligonucleotides more salt intolerant than smallerones
Effects of salt can be partially mitigated by choiceof buffers See Griffey et al. RCMS 1995; 9; 97-102.
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Salt is a KillerESI-MS of 20-mer phosphorothioate oligonucleotide
500 700 900 1100 1300 m/z0
1 x 106
500 700 900 1100 1300 m/z0
2.1 x 107
Intensity
Intensity
1 mM Na+
10 M Na+
1050 10901050 1090
1050 10901050 1090
MW?
MW
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non-adducted mass spectrum
Well F01Q:\roboticsdata\archive\completed\P00005563\61\acqus
865 870.52 876.06 881.62 887.19 892.78 898.39 904.02 909.66 915.32 921
m/z0.00
16545.5
33091
49636.5
66182
Well F12Q:\roboticsdata\archive\completed\P00005563\72\acqus
865 870.52 876.06 881.62 887.19 892.78 898.39 904.02 909.66 915.32 921
m/z
9635.5
19271
28906.5
38542
48177.5
57813
67448.5
77084
Adducted
Not adducted
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Mass Analyzers
All work by measuring the response of chargedparticles to electric and/or magnetic fields
All work at reduced pressure to reduce ion-neutralcollisions
Want to minimize scatter and/or neutralization
Typical operating pressures
Linear quadrupoles ~ 5 x 10-5 torr
FTICR < 10-9 torr TOF 10-5 10-7 torr
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Highlights of TOF-MS Advantages:
Simple and rugged benchtop construction
Theoretically unlimited mass range
Adaptable to many ionization sources
Fast acquisition - signal averaging to improve S/N
Mass accuracy rivals that of FTICR Disadvantages:
Limited resolution
Theoretically limited to detection electronics
Practically limited by energy and spatial spreads in ions
TOF is inherently pulsed Must wait for longest flight time ions before sending next packet of
ions (Hz to kHz typical repetition rates)
Cannot simultaneously measure all m/zvalues
This is mitigated by external ion accumulation
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Time-of-flight (TOF) Mass Analyzers
Ions are accelerated by electric field (V/d)
Ions then drift at their final velocity for a fixed distance
Ions impact a detector and their flight time is recorded
flight time is
proportional to velocity
proportional to the square root of m/z
dVvz
mmvEK /
2
1
2
1..
22 =
=
t = L/ = L m/2zVt: sec L: meters : velocity m: kg z: Coulombs V: voltslower m/zions reach higher velocity than higher m/zions
where is velocity, V/d is field strength
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TOF-MS Detection Schemes Particle impact, electron generation, and detection
Electron Multiplier
Microchannel Plate
Hybrids or Other particle detectors
Simplest example: metal foil
Most common: microchannel plate
Array of tilted glass channels 2-10 microns
Electron cascade=gain
Also used in night vision
ion Electrons (a few)
ion 106
- 1012
electrons
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Mass Analyzers - TOF
Linear Geometry Ions drift in field-free region, but energy spread (+E)
leads to time spread (-T) (more energy gives shorterTOF)
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Mass Analyzers - TOF Reflectron
Ions drift, but at ion mirror they turn around
+E (energy spread) leads to deeper penetration in ionmirror
Linear config: +E leads to -T Reflectron config: +E leads to -T+T (=0; energy spread
eliminated at detector)
Diagram for single m/zion withenergy difference
E+E
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ESI with an External Ion Reservoir ESI is a continuous ionization source while most MS
platforms are most effectively coupled to pulsed sources Couple external ion reservoir with ESI to make a pulsed
ionization source
Nearly 100% ionization duty cycle
Ions are externally accumulated while others are being mass
analyzed
skimmercone
rf-only hexapole
gateelectrode
inletcapillary
turboPump
ESIplume
roughpump
turbodragpump
coldcathodegauge
heatedcounter-currentgas flow
To MS
skimmercone
rf-only hexapole
gateelectrode
inletcapillary
turboPump
ESIplume
roughpumproughpump
turbodragpump
coldcathodegauge
heatedcounter-currentgas flow
To MS
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Mass Spectrometry and T5000
Profile 1
Profile 2
Profile 3
Forensic profile compared with existing databaseentries, or used to populate database
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Conclusions In general, mass spectrometry is used to weigh molecular
analytes of interest
Electrospray ionization is employed as it can promote large,intact oligonucleotides into the gas phase
Time-of-Flight mass spectrometry is used as it providesaccurate molecular weight measurements in a robust,benchtop, instrument format
As part of the Ibis process, amplified DNA is weighed with
enough accuracy to unambiguously determine basecomposition [AGCT]
Base composition profiles can be compared to other profilesand/or databases
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Abbreviations and Jargon
APCI atmospheric pressure chemical ionization
bp base pair(s)
CAD collisionally activated dissociation
Da Dalton = atomic mass unit
DNA deoxyribonucleic acid
Ds double stranded (DNA)
EI electron impact (ionization)
ESI electrospray ionization
FAB fast atom bombardment
FD field desorption (ionization)
FI field ionization
FTICR Fourier transform ion cyclotron resonance
FTMS Fourier transform mass spectrometry
FWHM full width half maximum (used to specify resolution)
GC gas chromatography
Hz Hertz (cycles/second)
IRMPD infrared multiphoton dissociation
kDa kilo Dalton(s)
m/m mass divided by peak width (mass resolution)m/z mass to charge ratio
MALDI matrix assisted laser desorption ionization
MSAD multipole storage assisted dissociation
mtDNA mitochondrial deoxyribonucleic acid
MW molecular weight
PCR polymerase chain reaction
PD plasma desorption
ppm parts per million
QIT quadrupole ion trap
Q-TOF quadrupole-time-of-flight
rf radio frequency
SIMS secondary ion mass spectrometry
ss single stranded (DNA)
TOF time-of-flight
TSP thermospray (ionization)
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Contact Information:
Steven A. Hofstadler, Ph.D.
Ibis Biosciences, Inc.
Email: [email protected]
mailto:[email protected]:[email protected]